Authors :
C. Keza; N. Mariita; A. Mwangi; J. C. Niyonzima; N. Nsengiyumva
Volume/Issue :
Volume 10 - 2025, Issue 1 - January
Google Scholar :
https://tinyurl.com/34ehems9
Scribd :
https://tinyurl.com/39jmkkrw
DOI :
https://doi.org/10.5281/zenodo.14890823
Abstract :
The geothermal energy sector in Burundi has not yet had any particular attention in term of developing this
renewable resource which has the potential as a source for electricity generation and direct use applications. The country
has more than 13 geothermal springs spread over different regions. This research is focused on the characterization of
geothermal reservoir of Mugara and Ruhwa sites. Geophysical and geochemical methods have been used to collect the
data. Thus, geological, electrical resistivity data based to Schlumberger method and chemical elements were analysed in
order to investigate the geological structures and the quality of these geothermal reservoirs. The results showed that in
Mugara site, the geothermal reservoir is located geologically in the spongoliths, coarse cemented sands, clay-sandstone
spongoliths whereas the Ruhwa site is found in the white quartzites with intercalations of phyllite rocks with the presence
of schites, psammoshistose, sandstone-silty quartzites. The aquifer in Mugara site is a semi-confined aquifer and the
Ruhwa geothermal reservoir is a confined aquifer due to its roof, which is composed of clay. The highest temperature in
Ruhwa site is 68°c and underground source temperatures are postulated to be as high as 110-120°c based on the quartz
geothermometer in the hot springs from the porous sediments. The chemical analysis results of water from Ruhwa and
Mugara indicated that 3 elements which are Fe, Mg and K have a high content of 21.5 mg/l, 10mg/l and 76mg/l
respectively.
Keywords :
Geothermal Reservoir, Burundi, Resistivity, Geology, Ruhwa, Mugara.
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The geothermal energy sector in Burundi has not yet had any particular attention in term of developing this
renewable resource which has the potential as a source for electricity generation and direct use applications. The country
has more than 13 geothermal springs spread over different regions. This research is focused on the characterization of
geothermal reservoir of Mugara and Ruhwa sites. Geophysical and geochemical methods have been used to collect the
data. Thus, geological, electrical resistivity data based to Schlumberger method and chemical elements were analysed in
order to investigate the geological structures and the quality of these geothermal reservoirs. The results showed that in
Mugara site, the geothermal reservoir is located geologically in the spongoliths, coarse cemented sands, clay-sandstone
spongoliths whereas the Ruhwa site is found in the white quartzites with intercalations of phyllite rocks with the presence
of schites, psammoshistose, sandstone-silty quartzites. The aquifer in Mugara site is a semi-confined aquifer and the
Ruhwa geothermal reservoir is a confined aquifer due to its roof, which is composed of clay. The highest temperature in
Ruhwa site is 68°c and underground source temperatures are postulated to be as high as 110-120°c based on the quartz
geothermometer in the hot springs from the porous sediments. The chemical analysis results of water from Ruhwa and
Mugara indicated that 3 elements which are Fe, Mg and K have a high content of 21.5 mg/l, 10mg/l and 76mg/l
respectively.
Keywords :
Geothermal Reservoir, Burundi, Resistivity, Geology, Ruhwa, Mugara.